Research progress of monitoring for dripping water environment in karst caves

PENG Ling-li; LI Ting-yong

doi:10.3969/j.issn.1001-4810.2012.03.014

Volume 31 Issue 3

Sep. 2012

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PENG Ling-li, LI Ting-yong. Research progress of monitoring for dripping water environment in karst caves[J]. CARSOLOGICA SINICA, 2012, 31(3): 316-326. doi: 10.3969/j.issn.1001-4810.2012.03.014

Citation:

PENG Ling-li, LI Ting-yong. Research progress of monitoring for dripping water environment in karst caves[J]. CARSOLOGICA SINICA, 2012, 31(3): 316-326. doi: 10.3969/j.issn.1001-4810.2012.03.014

PENG Ling-li, LI Ting-yong. Research progress of monitoring for dripping water environment in karst caves[J]. CARSOLOGICA SINICA, 2012, 31(3): 316-326. doi: 10.3969/j.issn.1001-4810.2012.03.014

Citation:

PENG Ling-li, LI Ting-yong. Research progress of monitoring for dripping water environment in karst caves[J]. CARSOLOGICA SINICA, 2012, 31(3): 316-326. doi: 10.3969/j.issn.1001-4810.2012.03.014

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Research progress of monitoring for dripping water environment in karst caves

doi: 10.3969/j.issn.1001-4810.2012.03.014

PENG Ling-li¹,
LI Ting-yong²

1.
School of Geographical Sciences, Southwest University/Key Laboratory of Eco-Environments in Three Gorges Reservoir Region, Ministry of Education
2.
School of Geographical Sciences, Southwest University/Key Laboratory of Eco-Environments in Three Gorges Reservoir Region, Ministry of Education；Institute of Earth Environment, CAS / State Key Laboratory of Loess and Quaternary Geology

Received Date: 2012-02-26
Publish Date: 2012-09-25

Abstract

Abstract

Based on the study of the former achievement, it is concluded that the research process of monitoring for dripping water environment in karst caves mainly includes the following5 items.(1) Although the oxyhydrogen isotope component in dripping water basically represents the isotope components in the atmospheric precipitation, variation of the oxyhydrogen isotope in dipping water is diversity, due to the differences in the thickness and fissures of the overlying rocks above the cave, that leading to the differences in time response between the dripping water and the rainfall.(2) The chemical component of the dripping water mainly affected by the interaction among water, soil, bedrock and gas, and the dissolved inorganic carbon and organic acid is also affected by the vegetation form and density.(3) The physical condition of caves is an important factor that deciding whether the oxygen and carbon stable isotopes in the speleothem by dripping water can reach the state of equilibrium fractionation or not.(4)Because there are multiple solution and uncertainty in the indicating climatic change by components of the dripping water, the cave monitor should be extended to the overlying soil and vegetation outside of the cave to form a three-dimensional monitor system.(5) Mmonitoring for karst cave environments still needs synthetic comparison study under different natural conditions.
- dripping water in caves,
- climatic environment,
- hydrochemistry,
- carbon and oxygen stable isotope

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References(89)

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Research progress of monitoring for dripping water environment in karst caves

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